摘要
在总结已有的饱和非饱和渗流模型的基础上,把裂隙岩体看作是离散网络模型,分析研究了含节理裂隙岩体的非饱和渗流特性,建立了裂隙网络饱和非饱和渗流模型,并推导了控制方程.对节理裂隙岩体中外力对裂隙渗流的影响进行了分析研究,提出了渗流场应力场耦合的分析模型,推导出三维应力与裂隙水压力共同作用下一组平行裂隙组的渗流应力耦合关系式.
Based on saturated seepage flow and unsaturated seepage flow model,using the fracture network model,the unsaturated seepage flow characteristics of crack rock mass are analyzed,and the constitutive relation is established.The influence of stress on seepage is analyzed,and the seepagestress coupling model is put forward.The seepagestress coupling relationship of parallel cracks under the action of three dimensional stresses and pore pressure is set up.
出处
《武汉化工学院学报》
2004年第4期44-48,共5页
Journal of Wuhan Institute of Chemical Technology
基金
国家自然科学基金项目(10072072)
国家自然科学重点基金项目(50334060)
关键词
裂隙岩体
渗流—应力耦合分析
非饱和渗流
fractured rock mass
seepagestress coupling analysis
unsaturated seepage